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学者姓名：王力圆
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Abstract ：
岩浆作用的不同时期、不同种属的碱性暗色矿物的矿物学信息能反演岩浆演化过程.本文对福建福州鼓山地区的晶洞花岗岩进行了主微量元素、锆石U-Pb同位素定年、Lu-Hf同位素分析,并对其特征暗色矿物进行了电子探针微区分析.鼓山花岗岩发育典型的钠铁闪石、霓石等碱性暗色矿物,地球化学特征表现为高硅、富碱、贫镁钙、低铁铝,属于准铝质到过碱质岩石;其LREE富集,HREE亏损,具有Eu负异常的特征,均显示K、Rb、Th、U等元素相对富集,Ba、Sr以及高场强元素Nb、Ta、P、Ti相对亏损,为典型的高分异的碱性A型花岗岩.LA-ICP-MS锆石U-Pb年龄在95Ma左右,指示其形成时代为晚白垩世早期.锆石的平均ΔFMQ=+5.36,表明岩浆具有较高的氧逸度,钠铁闪石和霓石等碱性暗色矿物形成于岩浆演化的晚期阶段.霓石显示出其高硅、高钠、高铁,低钛、镁、铝、锰的特征.钠铁闪石具有富碱、高铁、多硅、贫钙的特征.碱性花岗岩的锆石εHf(t)值范围为-1.8～+5.4,二阶段模式年龄tDM2为810～1278Ma,岩浆源区为同期底侵的富集地幔来源的陆壳岩石在高温下部分熔融形成,形成于太平洋板块俯冲后撤背景下的伸展环境.
Keyword ：
A型花岗岩 A型花岗岩 岩石成因 岩石成因 福州鼓山 福州鼓山 钠铁闪石 钠铁闪石 霓石 霓石
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| GB/T 7714 | 邓心禾 , 王力圆 , 徐净 et al. 福州鼓山地区A型花岗岩中碱性暗色矿物特征及其地质意义 [J]. | 岩石学报 , 2025 , 41 (1) : 112-134 . |
| MLA | 邓心禾 et al. "福州鼓山地区A型花岗岩中碱性暗色矿物特征及其地质意义" . | 岩石学报 41 . 1 (2025) : 112-134 . |
| APA | 邓心禾 , 王力圆 , 徐净 , 陈素余 . 福州鼓山地区A型花岗岩中碱性暗色矿物特征及其地质意义 . | 岩石学报 , 2025 , 41 (1) , 112-134 . |
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The Ganfang district in the Yifeng County, Jiangxi Province is an important rare metalmetallogenic area. A series of Li-Rb rare metal deposits (mineralization) have been discovered in the Ganfang intrusions, while the mineralization mechanism of rare metals is not clear yet. The detailed mineralogy texture and composition of feldspars and micas from the Dongshang granite have been analyzed by electron microprobe analysis. The results show that micas are the main carriers of Rb (Rb2O <1.07%), and the contents of Rb in feldspars are lower (Rb2O <0.11%), particularly in albite. The Rb-bearing micas are mainly phengite to zinnwaldite from muscovite granite, pegmatite, and granitic aplite. The substituted mechanism of Rb in micas is mainly coupled with Na for interlayer cation of K. The mineral textures record both magma crystallization differentiation and fluid metasomatism for the Dongshang granites, however, the former was the key mechanism of the Rb enrichment, while the later has less role on the accumulation of Rb in granites. Together with previous publications, this paper concluded that the Ganfang intrusions have a good metallogenic potential of rare metals, and the subsequent prospecting should focus on the Li, Rb, and other rare metals related to the Early Cretaceous to Late Jurassic (140~150 Ma) highly differentiated granites. © 2024 China Geological Survey. All rights reserved.
Keyword ：
Dongshang granite Dongshang granite Ganfang intrusions Ganfang intrusions granite granite Jiangxi Province Jiangxi Province mineral exploration engineering mineral exploration engineering rare metals rare metals Rb Rb
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| GB/T 7714 | Jiang, J. , Guo, X. , Xu, J. et al. Genesis of Rb mineralization of the Dongshang rare metal granite in Jiangxi Province; [江 西 甘 坊 洞 上 稀 有 金 属 花 岗 岩 中 铷 矿 化 特 征 及 成因机制] [J]. | Geological Bulletin of China , 2024 , 43 (1) : 86-100 . |
| MLA | Jiang, J. et al. "Genesis of Rb mineralization of the Dongshang rare metal granite in Jiangxi Province; [江 西 甘 坊 洞 上 稀 有 金 属 花 岗 岩 中 铷 矿 化 特 征 及 成因机制]" . | Geological Bulletin of China 43 . 1 (2024) : 86-100 . |
| APA | Jiang, J. , Guo, X. , Xu, J. , Tian, L. , Xiong, G. , Wang, L. et al. Genesis of Rb mineralization of the Dongshang rare metal granite in Jiangxi Province; [江 西 甘 坊 洞 上 稀 有 金 属 花 岗 岩 中 铷 矿 化 特 征 及 成因机制] . | Geological Bulletin of China , 2024 , 43 (1) , 86-100 . |
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江西省宜丰县甘坊地区是一个重要的稀有金属成矿区，目前在甘坊岩体内发现了一系列锂铷稀有多金属矿床（点），但其成矿机制尚不明确。选择甘坊岩体内洞上花岗岩作为研究对象，采用电子探针技术对多种花岗岩中的长石和云母类矿物进行了精细的结构和成分分析。结果表明，云母类矿物是铷的主要载体（Rb_2O <1.07%），长石类矿物中Rb含量低（Rb_2O <0.11%），尤其是在钠长石中Rb的含量几乎为0。含铷云母主要是白云母花岗岩、伟晶岩和细晶岩中的多硅白云母-铁锂云母类，其中铷可能主要通过与钠双置换云母结构中的层间钾离子存在。矿物结构特征显示，洞上花岗岩经历了明显的岩浆结晶分异和流体交代作用。结晶分异作用可能是洞上花岗岩Rb富集成矿的关键机制，而后期流体交代蚀变过程对铷的聚集作用有限。结合前人研究成果，笔者认为甘坊地区具有较好的锂、铷等稀有金属成矿潜力，后续的找矿勘查应注重与早白垩世—晚侏罗世（140～150Ma）高分异花岗岩相关的锂、铷等稀有金属矿床的找矿工作。
Keyword ：
江西 江西 洞上花岗岩 洞上花岗岩 甘坊岩体 甘坊岩体 矿产勘查工程 矿产勘查工程 稀有金属 稀有金属 花岗岩 花岗岩 铷 铷
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| GB/T 7714 | 姜军胜 , 郭欣然 , 徐净 et al. 江西甘坊洞上稀有金属花岗岩中铷矿化特征及成因机制 [J]. | 地质通报 , 2024 , 43 (01) : 86-100 . |
| MLA | 姜军胜 et al. "江西甘坊洞上稀有金属花岗岩中铷矿化特征及成因机制" . | 地质通报 43 . 01 (2024) : 86-100 . |
| APA | 姜军胜 , 郭欣然 , 徐净 , 田立明 , 熊光强 , 王力圆 et al. 江西甘坊洞上稀有金属花岗岩中铷矿化特征及成因机制 . | 地质通报 , 2024 , 43 (01) , 86-100 . |
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Iron, Cu, Pb-Zn, and W-Mo skarn deposits occur in the Gangdese metallogenic belt, Tibet. A lack of precise age constraints for mineralization hinders understanding of the processes contributing to skarn mineralization, particularly identification of the causative intrusions. In this study, new garnet U-Pb geochronological data are provided for the Qiagong (Fe) and Jiaduobule (Fe-Cu) skarns. We place particular emphasis on skarn garnet mineralogy, using scanning electron microscopy (SEM), electron probe microanalysis (EPMA), and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), to characterize garnet textures, compositions, and U-Pb isotope systematics. All garnets studied belong to the grossular-andradite series and display oscillatory compositional zoning (And 100 Gr 0 to And 20 Gr 80 ). Andradite-dominated garnet features a chondrite-normalized REE fractionation pattern exhibiting enrichment in LREE relative to HREE and a positive Eu anomaly, whereas grossular-dominated garnet displays relative LREE depletion and a marked flat HREE fractionation trend. Ore-forming elements, including Sn, W, As, and U, are detected at concentrations up to several hundreds of ppm in the same garnets. Concentrations of W and As are higher in andradite and correlate positively with one another. The correlation between U, Sn and the major oxide composition of garnet is insignificant, potentially resulting from the changing valence states of these elements under different redox conditions. Together with previously published and limited new data for the Gebunongba (Fe), Ri'a (Cu), and Hahaigang (W-Mo) skarns, the new garnet U-Pb age data indicate that the major Fe, Pb-Zn, and W-Mo mineralization event in the Gangdese metallogenic belt took place between 65 Ma and 50 Ma, with marked peaks at - 65 Ma and - 53 Ma. Partial melting of a crustal-dominated source due to the slab rollback (-65 Ma) and break off (-53 Ma) of Yarlug-Zangbo Tethyan Ocean and subsequent asthenosphere upwelling induced this regional event during the Paleogene to early Eocene. A less common but regionally widespread Cu (+/- Au) mineralization event in the same belt formed during the Late Cretaceous (-85 Ma) and may have resulted from the coupled influence of the northward subduction of the Yarlug-Zangbo Tethyan Ocean and the southward subduction of the Bangong-Nujiang Tethyan Ocean. This contribution highlights the potential significance of the Late Cretaceous Cu(+/- Au) event and hence the prospectivity of the belt for both skarn and porphyry systems. More broadly, our findings carry implications for Neo-Tethyan metallogeny in the region extending from southwestern China to eastern Europe during the Late Cretaceous. (c) 2024 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
Keyword ：
Gangdese belt Gangdese belt Garnet Garnet LA-ICP-MS LA-ICP-MS Skarn Skarn Tibet Tibet U-Pb geochronology U-Pb geochronology
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| GB/T 7714 | Xu, Jing , Li, Jiadai , Cook, Nigel J. et al. Redefining timing, genesis and geodynamic setting of polymetallic skarn mineralization, Gangdese belt, Tibet, from LA-ICP-MS garnet U-Pb geochronology [J]. | GONDWANA RESEARCH , 2024 , 132 : 113-135 . |
| MLA | Xu, Jing et al. "Redefining timing, genesis and geodynamic setting of polymetallic skarn mineralization, Gangdese belt, Tibet, from LA-ICP-MS garnet U-Pb geochronology" . | GONDWANA RESEARCH 132 (2024) : 113-135 . |
| APA | Xu, Jing , Li, Jiadai , Cook, Nigel J. , Ciobanu, Cristiana L. , Wu, Shitou , Wade, Benjamin P. et al. Redefining timing, genesis and geodynamic setting of polymetallic skarn mineralization, Gangdese belt, Tibet, from LA-ICP-MS garnet U-Pb geochronology . | GONDWANA RESEARCH , 2024 , 132 , 113-135 . |
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Tin-bearing magnetite is reported from several types of magmatic-hydrothermal ore deposits. The question of whether tin is incorporated within solid solution, as Sn4+, or as nanoinclusions remains open, however. We report a micron- to nanoscale investigation of Sn (Mg, Si)-bearing magnetite from serpentinite in the Dulong Zn-Sn-In skarn, South China, with the dual aims of understanding the mechanisms involved in accommodating Sn and associated elements into the Fe-oxide, and the inferences that this carries for constraining the early stages of skarn formation. Magnetite preserves a range of textures that record the evolution of metasomatism during prograde growth of grain cores and retrograde rim replacement. Observations reveal the presence of chondrodite and sellaite (MgF2) as nanoscale inclusions preserved in magnetite. This implies initiation of the Dulong mineralizing system during a humite-bearing, magnesium skarn stage. Magnesium-Si defects, forming along (110) planes prior to Sn-enrichment, are recognized for the first time. Release of high volatile, F-rich fluids is interpreted to lead to precipitation of cassiterite inclusions along < 111*> directions in magnetite.
Keyword ：
cassiterite cassiterite crystal structure crystal structure Dulong Dulong HAADF STEM HAADF STEM humite group humite group magnetite magnetite skarn skarn
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| GB/T 7714 | Xu, Jing , Ciobanu, Cristiana L. , Cook, Nigel J. et al. Tin-bearing magnetite with nanoscale Mg-Si defects: Evidence for the early stages of mineralization in a skarn system [J]. | FRONTIERS IN EARTH SCIENCE , 2023 , 10 . |
| MLA | Xu, Jing et al. "Tin-bearing magnetite with nanoscale Mg-Si defects: Evidence for the early stages of mineralization in a skarn system" . | FRONTIERS IN EARTH SCIENCE 10 (2023) . |
| APA | Xu, Jing , Ciobanu, Cristiana L. , Cook, Nigel J. , Slattery, Ashley D. , Ehrig, Kathy , Wade, Benjamin P. et al. Tin-bearing magnetite with nanoscale Mg-Si defects: Evidence for the early stages of mineralization in a skarn system . | FRONTIERS IN EARTH SCIENCE , 2023 , 10 . |
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对福建省沿海至内陆出露的4件新生代玄武岩进行40 Ar/39 Ar年龄测试,对玄武岩中橄榄石斑晶进行电子探针测试;其中洋底和柳城玄武岩首次获得精确的40 Ar/39 Ar年龄数据.结果显示,闽西明溪40 Ar/39 Ar年龄数据为(1.44±0.11)Ma,柳城为(17.35±0.93)Ma;闽中洋底玄武岩年龄为(11.71±0.44)Ma;闽东厦门玄武岩年龄为(17.0±0.36)Ma.结合前人年龄数据,福建省新生代玄武岩整体表现出从闽东至闽西年龄逐渐减小的趋势.橄榄石斑晶电子探针数据显示闽东至闽西玄武岩碱性程度逐渐增加,可能指示岩浆熔融程度由沿海至内陆逐渐减少,岩石圈厚度由东向西逐渐增厚.最新获得的闽西柳城玄武岩40Ar-39Ar年龄为(17.35±0.93)Ma,与东部沿海玄武岩相似,推测可能是太平洋板块北西向俯冲时引起的岩浆扰动作用形成的.
Keyword ：
40 Ar/ 39 Ar年龄 40 Ar/ 39 Ar年龄 地质意义 地质意义 新生代玄武岩 新生代玄武岩 橄榄石斑晶 橄榄石斑晶 福建省 福建省
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| GB/T 7714 | 严率旗 , 张文慧 , 王力圆 et al. 福建省新生代玄武岩40Ar/39Ar年代学及地质意义 [J]. | 福州大学学报（自然科学版） , 2023 , 51 (1) : 118-124 . |
| MLA | 严率旗 et al. "福建省新生代玄武岩40Ar/39Ar年代学及地质意义" . | 福州大学学报（自然科学版） 51 . 1 (2023) : 118-124 . |
| APA | 严率旗 , 张文慧 , 王力圆 , 聂俊韬 . 福建省新生代玄武岩40Ar/39Ar年代学及地质意义 . | 福州大学学报（自然科学版） , 2023 , 51 (1) , 118-124 . |
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The Rb mineralization is associated -with rare metal granites. However, -widespread hydrothermal alteration in the late evolution of rare metal granites makes it difficult to distinguish the magmatic process from the hydrothermal process. It is still unclear whether the rare metal mineralization is dominated by magmatic differentiation or hydrothermal metasomatism. The Ganfang intrusion in the Jiangxi Province is an important rare metal metallogenic area, where a series of Li-Rb rare metal deposits (mineralization) have been discovered, and the mineralization mechanism of rare metals is not yet clear. This paper takes both granite-type Rb (Baiguo, Dagang, and Nanmukeng) and aplite-type Rb (Fuhua, Tongan) mineralization from the Ganfang intrusion for case studies. The detailed mineralogy texture and composition of feldspars and micas have been analyzed by automatic mineral scanning system, electron probe and LA-ICP-MS. The results show that micas are the main carriers of Rb (1683X10 -12047X10 ), and the contents of Rb in feldspars are lower. The Rb content of K-feldspar is 1683X10 -4051X10 , whereas albite contains almost no Rb concentration (1. 82 X 10 -89.94X10 ). The Rb-bearing micas transfer from muscovite, though Li-phengite and zinnwaldite, to lepidolite, in which substituted mechanisms for Li are 2Li + ,vSi4+- v,Al3++v,Al3++n andLi++Fe2+- V,A13++H, and for Rb is Rb+/ Na+ /Cs+ ~ K+. The mineral textures and compositions record both magma crystallization differentiation and fluid metasomatism for Ganfang granites; however, the former -was the key enrichment mechanism for Rb as •well as Li. © 2023 Geological Society of China. All rights reserved.
Keyword ：
enrichment mechanism enrichment mechanism Ganfang granite Ganfang granite granite granite Jiangxi Province Jiangxi Province rare metals rare metals Rb Rb
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| GB/T 7714 | Xu, J. , Hou, W. , Wang, L. et al. Rb mineralization during magmatic differentiation: Insight from mineralogical study on the Ganfang rare metal granite, Jiangxi Province; [稀有金属花岗岩结晶分异过程中铷的富集与成矿来自江西甘坊岩体的矿物学证据] [J]. | Acta Geologica Sinica , 2023 , 97 (11) : 3766-3785 . |
| MLA | Xu, J. et al. "Rb mineralization during magmatic differentiation: Insight from mineralogical study on the Ganfang rare metal granite, Jiangxi Province; [稀有金属花岗岩结晶分异过程中铷的富集与成矿来自江西甘坊岩体的矿物学证据]" . | Acta Geologica Sinica 97 . 11 (2023) : 3766-3785 . |
| APA | Xu, J. , Hou, W. , Wang, L. , Zhao, T. , Chen, S. , Tian, L. . Rb mineralization during magmatic differentiation: Insight from mineralogical study on the Ganfang rare metal granite, Jiangxi Province; [稀有金属花岗岩结晶分异过程中铷的富集与成矿来自江西甘坊岩体的矿物学证据] . | Acta Geologica Sinica , 2023 , 97 (11) , 3766-3785 . |
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The mafic microgranular enclaves (MMEs) from Mesozoic intermediate-acid magmatic rocks, widely developed along the Fujian coast, are considered to be the results of large-scale crust- mantle interaction by magma mixing. This paper is based on zircon U-Pb chronology, along with zircon Hf isotope and mineral analyses for the host granite and MMEs from Langqi Island, in order to investigate the magma mixing mechanism of the Langqi pluton in Fuzhou, Southeast China. The results indicate that the MMEs were emplaced during the late Early Cretaceous (98.9 +/- 2.2 Ma), identical to the age of the granite (100.1 +/- 1.1 Ma) within the error range. The zircon epsilon Hf(t) values for the granite and MMEs are in the ranges of -2.1 similar to 0.0 and-1.7 similar to+1.1. The zircon Hf isotope data indicate that both the granite and MMEs were predominantly derived from the ancient crustal basement of Cathaysia, with a partial mantle-derived contribution. The An values of plagioclase phenocrysts with oscillatory zoning patterns in the MMEs show oscillatory changes from the core to the rim, indicating multiple mixing events between the two magmas with different compositions. Amphiboles in the MMEs show characteristics of crust-mantle contamination, and the Ti migrated from the mafic magma with high concentration to the felsic magma with low concentration during the magma mixing process. Biotites in the host rock and MMEs belong to primary biotite, and they have relatively high MgO contents (ave. 12.78 wt.%) and relatively low FeOT/(MgO + FeOT) ratios (ave. 0.56), showing characteristics of crust-mantle contamination. The crust-mantle magma interaction in a crystal, mushy state played a significant role in controlling the formation and evolution of the Langqi pluton. The magmatism was predominantly sourced from mixing between the mantle-derived mafic magma and the crust-derived felsic magma during the subduction of the Paleo-Pacific Plate, resulting in the formation of the Langqi doleritic veins, granites, and MMEs.
Keyword ：
chronology chronology Langqi Island Langqi Island mafic microgranular enclaves mafic microgranular enclaves magma mixing magma mixing mineralogy mineralogy
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| GB/T 7714 | Chen, Zhouxin , Wang, Liyuan , Yan, Xue . Chronological and Mineralogical Records of the Langqi Pluton, Fuzhou: Constraints on the Magma Mixing Process [J]. | MINERALS , 2023 , 13 (12) . |
| MLA | Chen, Zhouxin et al. "Chronological and Mineralogical Records of the Langqi Pluton, Fuzhou: Constraints on the Magma Mixing Process" . | MINERALS 13 . 12 (2023) . |
| APA | Chen, Zhouxin , Wang, Liyuan , Yan, Xue . Chronological and Mineralogical Records of the Langqi Pluton, Fuzhou: Constraints on the Magma Mixing Process . | MINERALS , 2023 , 13 (12) . |
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The Ediacaran glaciation has garnered considerable attention for its potential biological impact because it witnesses the birth of complex animals. Many researchers question whether large-scale regional or even global glaciations, represent critical barriers to the evolution of macroscopic animals. So how did complex animals survive during a major glaciation? One possible explanation is the existence of isolated shallower refugia or icefree oases. However, the sedimentary evolution of such ice-free oases and how they could support the survival of complex life forms are not yet fully understood. This study focuses on the inter-diamictite black sediments in the Ediacaran Talisayi Formation of NW China (Yili block), which may represent a habitable ice-free oasis during the Gaskiers glaciation. The sedimentary facies and geochemical analyses indicate that these deposits were formed in oxygenated and photic shallow glacier lake environments with highly developed microbial mat substrates, it was formed during a short-lived partial deglaciation with enhanced weathering. And diverse organic-wall microfossils were found within the inter-diamictite black sediments. Furthermore, based on the growth habits of modern microbial algal mats, a paleontological clock can be established to estimate the duration of partial deglaciation, which may have lasted only for thousands of years. The ice-free oasis formed during this period could potentially harbor complex ecosystems, providing valuable ecological and temporal windows for the evolution of complex animals.
Keyword ：
Ediacaran Ediacaran Gaskiers glaciation Gaskiers glaciation Ice free oasis Ice free oasis Microbial mat Microbial mat Partial deglaciation Partial deglaciation
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| GB/T 7714 | Zhang, Xinsong , An, Yanqing , Chen, Yarui et al. Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases" [J]. | PRECAMBRIAN RESEARCH , 2023 , 401 . |
| MLA | Zhang, Xinsong et al. "Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases"" . | PRECAMBRIAN RESEARCH 401 (2023) . |
| APA | Zhang, Xinsong , An, Yanqing , Chen, Yarui , Du, Weidong , Wang, Liyuan . Microbial mat, organic-wall microfossils and geochemistry of the Ediacaran inter-diamictite black sediments in NW China: A short-lived habitable benthic, oxic and photic "ice-free oases" . | PRECAMBRIAN RESEARCH , 2023 , 401 . |
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作为研究洋壳俯冲和壳幔相互作用理想对象的新生代玄武岩在福建省从沿海至内陆均有分布，根据地理位置这些新生代玄武岩可分成闽西、闽中与闽东沿海三个区域。本文对这些玄武岩进行了系统的全岩主、微量元素以及Sr、Nd、Pb、Hf同位素研究。结果表明，这些新生代玄武岩主要为碱性玄武岩、碧玄岩和粗面玄武岩，结合前人研究资料，可见这些玄武岩自闽东向闽西具有年龄逐渐变小、碱性逐渐增加的趋势。Sr、Nd、Pb、Hf同位素揭示这些玄武岩具有亏损地幔(DMM)与EMⅡ型富集地幔组分混合的特征。闽东沿海玄武岩相较于闽西、闽中玄武岩具有更高的Sr、Pb含量，更低的~(143)Nd/~(144)Nd值和~(176)Hf/~(177)Hf值，更趋近于EMⅡ特征。从西至东富集组分EMⅡ的逐渐增多暗示陆源沉积物与俯冲效应有关，这些陆源沉积物极可能是由俯冲洋壳带入软流圈地幔的。整个新生代玄武岩的Zr、Hf、Ti负异常与Pb同位素组成特征指示俯冲沉积物中可能含有碳酸盐组分。闽中柳城地区玄武岩的喷发年龄与闽东沿海地区玄武岩的喷发年龄较为接近；闽中柳城地区玄武岩Sr、Nd、Pb、Hf同位素特征与闽中其他玄武岩的一致，这可能与太平洋板块俯冲导致的大陆边缘上地幔发生补偿性的隆起有关；柳城地区玄武岩具有较低的SiO_2含量及最高的CaO/Al_2O_3值，可能是源区受到俯冲再循环碳酸盐组分影响的结果。
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同位素 同位素 微量元素 微量元素 新生代玄武岩 新生代玄武岩 福建省 福建省
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| GB/T 7714 | 严率旗 , 张文慧 , 王力圆 et al. 福建省新生代玄武岩成因:Sr、Nd、Pb、Hf同位素地球化学约束 [J]. | 矿物岩石地球化学通报 , 2023 , 42 (03) : 588-601 . |
| MLA | 严率旗 et al. "福建省新生代玄武岩成因:Sr、Nd、Pb、Hf同位素地球化学约束" . | 矿物岩石地球化学通报 42 . 03 (2023) : 588-601 . |
| APA | 严率旗 , 张文慧 , 王力圆 , 聂俊韬 . 福建省新生代玄武岩成因:Sr、Nd、Pb、Hf同位素地球化学约束 . | 矿物岩石地球化学通报 , 2023 , 42 (03) , 588-601 . |
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